A. Gerecke et al., THE CHEMICAL-KINETICS OF HONO FORMATION RESULTING FROM HETEROGENEOUS INTERACTION OF NO2 WITH FLAME SOOT, Geophysical research letters, 25(13), 1998, pp. 2453-2456
Uptake experiments at ambient temperature of NO2 on ethylene, acetylen
e and toluene soot resulted in significant amounts of MONO. The initia
l uptake coefficient gamma(0) of NO2 on ethylene soot decreased from 0
.12 to 0.03 with increasing NO2 concentration in the range 8 x 10(10)
to 1.4 x 10(13) molecule s(-1). The HONO yields relative to NO2 taken
up were in the range 50 to 93% and were consistent with a mechanism in
which either soot or hydrogen contained in it was the reducing agent.
The branching ratio of the yield of HONO and NO was a function of the
sampling spot at which the soot was collected within a diffusion flam
e and ranged from 23 to 2.2 with increasing distance from the flame ba
se and thus age. The total amount of HONO generated in one uptake expe
riment was 1.2 x 10(16) molecules per mg of soot. Heating cycles bring
back the ability of soot to generate MONO, but at diminishing yields.